Multi-stage evolution of xenotime-(Y) from Písek pegmatites,
Czech Republic: an electron probe micro-analysis and Raman
spectroscopy study

J 2016

Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study

ŠVECOVÁ, Eva, Renata ČOPJAKOVÁ, Zdeněk LOSOS, Radek ŠKODA, Lutz NASDALA et. al.

Basic information

Original name

Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study

Authors

ŠVECOVÁ, Eva (203 Czech Republic, belonging to the institution), Renata ČOPJAKOVÁ (203 Czech Republic, belonging to the institution), Zdeněk LOSOS (203 Czech Republic, guarantor, belonging to the institution), Radek ŠKODA (203 Czech Republic, belonging to the institution), Lutz NASDALA (40 Austria) and Jaroslav CÍCHA (203 Czech Republic)

Edition

Mineralogy and Petrology, 2016, 0930-0708

Other information

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10500 1.5. Earth and related environmental sciences

Country of publisher

Austria

Confidentiality degree

není předmětem státního či obchodního tajemství

Impact factor

Impact factor: 1.236

RIV identification code

RIV/00216224:14310/16:00090870

Organization unit

Faculty of Science

DOI

http://dx.doi.org/10.1007/s00710-016-0442-6

UT WoS

000388834300004

Keywords (in Czech)

xenotim-(Y); vodné roztoky; metamiktizace; rekrystalizace; alterace; EPMA; Ramanova spektroskopie

Keywords in English

xenotime-(Y); aqueous fluids; metamictization; recrystallization; alteration; EPMA; Raman spectroscopy

Abstract

V originále

The chemical variability, degree of radiation damage, and alteration of xenotime from the Písek granitic pegmatites (Czech Republic) were investigated by micro-chemical analysis and Raman spectroscopy. Dominant large xenotime–(Y) grains enriched in U, Th and Zr crystallized from a melt almost simultaneously with zircon, monazite and tourmaline. Xenotime is well to poorly crystalline depending on its U and Th contents. It shows complex secondary textures cutting magmatic growth zones as a result of its interaction with F, Ca, alkali-rich fluids during the hydrothermal stage of the pegmatite evolution.

Links

EE2.3.20.0052, research and development project

Name: Výzkumný tým pro ukládání radioaktivních odpadů a jadernou bezpečnost

Citovat

ŠVECOVÁ, Eva, Renata ČOPJAKOVÁ, Zdeněk LOSOS, Radek ŠKODA, Lutz NASDALA and Jaroslav CÍCHA. Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study. Mineralogy and Petrology. 2016, vol. 110, No 6, p. 747-765. ISSN 0930-0708. Available from: https://dx.doi.org/10.1007/s00710-016-0442-6.

@article{1354605,
   author = {Švecová, Eva and Čopjaková, Renata and Losos, Zdeněk and Škoda, Radek and Nasdala, Lutz and Cícha, Jaroslav},
   article_number = {6},
   doi = {http://dx.doi.org/10.1007/s00710-016-0442-6},
   keywords = {xenotime-(Y); aqueous fluids; metamictization; recrystallization; alteration; EPMA; Raman spectroscopy},
   language = {eng},
   issn = {0930-0708},
   journal = {Mineralogy and Petrology},
   title = {Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study},
   volume = {110},
   year = {2016}
}

TY  - JOUR
ID  - 1354605
AU  - Švecová, Eva - Čopjaková, Renata - Losos, Zdeněk - Škoda, Radek - Nasdala, Lutz - Cícha, Jaroslav
PY  - 2016
TI  - Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study
JF  - Mineralogy and Petrology
VL  - 110
IS  - 6
SP  - 747-765
EP  - 747-765
SN  - 09300708
KW  - xenotime-(Y)
KW  - aqueous fluids
KW  - metamictization
KW  - recrystallization
KW  - alteration
KW  - EPMA
KW  - Raman spectroscopy
N2  - The chemical variability, degree of radiation damage, and alteration of xenotime from the Písek granitic pegmatites (Czech Republic) were investigated by micro-chemical analysis and Raman spectroscopy. Dominant large xenotime–(Y) grains enriched in U, Th and Zr crystallized from a melt almost simultaneously with zircon, monazite and tourmaline. Xenotime is well to poorly crystalline depending on its U and Th contents. It shows complex secondary textures cutting magmatic growth zones as a result of its interaction with F, Ca, alkali-rich fluids during the hydrothermal stage of the pegmatite evolution.
ER  -

ŠVECOVÁ, Eva, Renata ČOPJAKOVÁ, Zdeněk LOSOS, Radek ŠKODA, Lutz NASDALA and Jaroslav CÍCHA. Multi-stage evolution of xenotime-(Y) from Písek pegmatites, Czech Republic: an electron probe micro-analysis and Raman spectroscopy study. \textit{Mineralogy and Petrology}. 2016, vol.~110, No~6, p.~747-765. ISSN~0930-0708. Available from: https://dx.doi.org/10.1007/s00710-016-0442-6.

Detailed Information on Publication Record